Download building stones of the brooklyn college campus

BUILDING STONES OF THE
BROOKLYN COLLEGE CAMPUS
Wayne Powell
LEARNING OBJECTIVES:
• Students will be able to differentiate between crystals and clastic grains
• Students will be able to identify common fossils with the aid of photographs.
• Students will be able to identify common rock fabrics.
• Students will be able to identify rocks commonly used for building stone, and document
the evidence
PREREQUISITE KNOWLEDGE AND SKILLS:
• Minerals lab
PRE-LAB PREPARATION:
• Read the material leading to the assignment
MATERIALS FOR STUDENTS TO BRING:
• A magnifying glass will be useful.
Copyright © 2007 Wayne Powell
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Rocks and Stones
A rock is a natural material that is composed of an aggregate of one or more minerals (naturally occurring, solid,
inorganic, crystalline substances), or organic materials (e.g., coal). A stone is a piece of rock that is used for a
specified function. Accordingly, the outcrops of marble in the southern Bronx neighborhood of Kingsbridge are
referred to as rock, whereas the grave markers in Lower Manhattan’s Trinity churchyard that were carved from this
material in the 1700’s are referred to as stone (gravestones).
Rocks are subdivided into three broad families based on the general processes and environments of formation:
•
Sedimentary Rocks form from the settling of eroded materials at the surface, most commonly under water.
This group includes clastic sedimentary rocks that are composed of weathered pieces of pre-existing rock
(e.g., sandstone), and chemical sedimentary rock that form from the precipitation of minerals from solution
(e.g., limestone). When grains settle they may form layers, or beds, that may be defined by differences in
color or grain size (see Examples of Rock Fabrics plate). This layering is called bedding.
•
Igneous Rocks form from the solidification of molten rock. Plutonic (intrusive) igneous rocks cool slowly,
deep within the Earth, and so exhibit large crystals. In contrast, volcanic (extrusive) igneous rocks cool
quickly after they have erupted to the surface from volcano, and so do not have crystals that are large
enough to be seen without a microscope. Most volcanic rocks make poor building stone because they may
be weak, cracked, inconsistent in color, and/or contain large pores. Accordingly, volcanic rocks will not be
discussed further in this lab.
•
Metamorphic Rocks form from the recrystallization and deformation of pre-existing rocks due to extreme
heat and pressure. The directed pressure that is commonly associated with metamorphism reorients and
rearranges mineral grains. This may result in the alignment of long or flat minerals to define a foliation (see
Examples of Rock Fabrics plate). Under more extreme metamorphic conditions the minerals may segregate
into distinct light and dark colored bands, forming a rock called gneiss (see Examples of Rock Fabrics
plate). Metamorphism may also deform banding in rocks to form folded patterns (see Examples of Rock
Fabrics plate).
The list of rocks that commonly have qualities that are suitable for building stone is relatively short, and is
summarized in the table below:
Rock
Family
Rock Name
Sedimentary
Sandstone
Reddish Brown,
White, Grey
Limestone
Grey, Beige
Grainy. Fossils are common. Bedding is common
White, Pink, Speckled
Crystalline. Crystals large enough to see. Light
colored
“Salt and Pepper”
Crystalline. Crystals large enough to see.
Gabbro
Black, Green, Dark Grey
Crystalline. Crystals large enough to see. Dark
colored
Marble
White, Pink
Crystalline. Wispy textures are
Stylolites are common. No fossils.
Gneiss
Pink, Black and White
Crystalline. Bands of distinctly different color.
Bands may be irregular and folded.
Igneous
Granite
Granodiorite
Metamorphic
Common Colors
Beige,
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Common Features
Grainy; composed of rounded grains up to 2 mm
in diameter. “Sandy” feel. Bedding is common.
common.
Crystals and Grains
Since rocks are aggregates of mineral grains, it is logical that the rocks will be differentiated/classified based upon
which minerals are present, and how the mineral components are arranged. The most important distinction in terms
of the arrangement of the minerals is the distinction between crystals (found in igneous and metamorphic rocks) and
sedimentary grains. Crystals are produced by the growth/replication of a regular, ordered arrangement of atoms.
Accordingly, crystals tend to have regular, polygonal shapes. Adjectives such as blocky, bladed, needle-like,
prismatic, rectangular, and hexagonal are commonly used to describe crystals. Sedimentary grains are formed by
forces acting on minerals. Abrasion due to transport of sedimentary grains tends to break off sharp edges, producing
spherical or ellipsoidal grains; sandstone is a sedimentary rock that is composed of small (<2mm diameter) rounded
grains. Fracture and collapse of rock tends to form irregular, angular fragments. Once cemented, these angular clasts
(rock fragments) form a rock called breccia. Biological activity may force minerals to grow into intricate shapes in
animal shells and skeleton. Such fossil grains can be recognized by complex, non-polygonal shapes such as spirals,
discs, and net-like structures.
Classification of Plutonic Igneous Rocks
Plutonic igneous rocks are classified based upon their chemical composition, which is reflected in their color. Rocks
that are low in iron and calcium are light in color and are composed predominantly of white and/or pink feldspars
and quartz. Rocks that are rich in iron and calcium are dark in color, and are composed predominantly of grey
feldspars and black or green minerals such as amphibole, pyroxene or olivine. Based on this simple color-based
scheme, three distinct plutonic rocks can be identified:
•
Granite: a light-colored (felsic) intrusive rock with crystals of quartz, white feldspar, pink feldspar, and mica
•
Granodiorite: an intermediately colored intrusive rock composed of light colored white to light grey feldspar
and dark green to black amphibole and/or biotite. The mix of light and dark minerals gives the rock a coarse
“salt-and-pepper” appearance.
•
Gabbro: a dark-colored (mafic) intrusive rock that consists of dark grey feldspar and black to dark green Ferich minerals such as amphibole and pyroxene.
Stone-workers and sculptors apply a different definition of granite. To them a granite is any hard rock that contains
crystals. These dual definitions of “granite” explain why, for example, the Brooklyn Museum of Art labels ancient
Egyptian sculptures that are carved from gabbro as being composed of “black granite”. To a geologist, the term
“black granite” would be an oxymoron, since by definition a granite must be light colored. A stone mason’s
definition of granite would also include the banded metamorphic rock called gneiss.
Limestone and Marble
Limestone is a sedimentary rock that is composed predominantly of the mineral calcite (calcium carbonate; CaCO3).
Most limestone forms in shallow, tropical, marine environments, and a common component of limestones are the
calcium carbonate skeletons of animals that live in these settings. Accordingly, limestones can often be identified by
the presence of marine fossils such as bivalves (e.g., clams), corals, and the coiled shells of gastropods (snails) (see
following photo plate). Other common fossil organisms that are less familiar to most people include bryozoans and
crinoids. Fossils of bryozoans commonly look like small pieces of lace or like a corkscrew (see following photo
plate). The most common fossil remains of crinoids are the discs that once comprised the stalk of this animal; in
rocks these fossils look like small buttons or poker chips (see following photo plate). Another distinct type of grain
that is common in limestone is an ooid, a BB-sized spherical or ellipsoidal grain that is composed of concentric
bands of calcite around a central sand grain (see Examples of Grainy Textures Plate). Ooids form in very shallow
marine environments where waves agitate and roll sand grains, allowing them to be coated on all sides by calcite
precipitates. As with other sedimentary rocks, limestones commonly exhibit the bedding.
Calcite is a relatively soluble mineral. (Remember that a diagnostic property of calcite is that it effervesces with
dilute acids.) Ground water seeping through limestone may result in local dissolution to form caves and caverns.
The weight of overlying rock may cause the roofs of such caves to collapse, filling the caves with broken pieces of
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limestone with irregular, angular shapes. When such deposits of broken rock are cemented together, they form a rock
called breccia in which the irregular, angular fragments are still evident (see Examples of Grainy Textures Plate).
Pressure increases the solubility of calcite, and so the burial of limestones may result in the formation of stylolites,
distinctive form of highly localized dissolution defined by a dark, irregular, zigzag discontinuity in the rock (see
Examples of Rock Fabrics plate).
If a limestone is deeply buried then it will metamorphose to become a marble. During the process of metamorphism,
the calcite (and/or dolomite) grains in the limestone will recrystallize, grow larger, and form crystals. Primary
features such as fossils and ooids are usually destroyed in this process, leaving a more uniform rock in which the
calcite occurs as polygonal, interlocking crystals that commonly have a sugary appearance. Layering such as bedding
or stylolites (see Examples of Rock Fabrics plate) that once existed in the limestone precursor may be deformed and
diffused, forming a wispy, “marbled” pattern (see Examples of Rock Fabrics plate).
To a geologist a marble is a metamorphosed limestone. However, to an architect, stone mason, or sculptor, a marble
is defined as any soft rock that will take a polish. This includes marbles, as well as densely-packed limestones, and
some less common rocks such as serpentinites. This difference in the specific meaning of the word “marble”
commonly leads to confusion. Some of the most common stones that are referred to as marble by builders, are
actually not metamorphosed and retain primary features such as fossils, ooids, and bedding. To determine whether a
polished soft rock is a true marble, you must examine the components and fabrics of the rock carefully. Are there
fossils or ooids that would indicate that it is a limestone? Are there angular fragments that would indicate that it is a
breccia? Or are there polygonal or sugary crystals of calcite, and wispy marbling that are characteristic of a true
marble?
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The Assignment
Station 1: Ingersoll Hall Foyer and Main Corridor
The foyer and main corridor immediately inside of the main doors of Ingersoll
Hall are lined with four examples of polished stone that would be classified as
marble by a stone mason or architect. The foyer contains a pinkish-tan stone on
the walls, and a pink-grey stone on the corners and decorative false columns.
The main corridor contains a medium grey stone on the walls and a deep pink
stone on the corners and decorative false columns.
Examine each of the three stones listed below and determine whether each of
these building stones is a limestone or a true marble (metamorphosed
limestone). Document your evidence and provide sketched of the diagnostic
features.
Main Corridor Grey Stone:
Limestone
Marble
(Circle One)
Supporting Evidence 1:
_______________________________________________________________________
Supporting Evidence 2:
_______________________________________________________________________
Supporting Evidence 3:
_______________________________________________________________________
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Foyer Pinkish-Tan Wall Stone:
Limestone
Marble
(Circle One)
Limestone
Marble
(Circle One)
Supporting Evidence 1:
____________________________
____________________________
Supporting Evidence 2:
____________________________
____________________________
Foyer Pink-Grey Corner Stone:
Supporting Evidence 1:
____________________________
____________________________
Supporting Evidence 2:
____________________________
____________________________
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Station 2: Ingersoll Extension Steps by the Lily Pond
Examine the components of the multi-colored rock that comprises the steps
to Ingersoll Extension. What are the grains? Sketch characteristic grains.
Pebbles
Fossils
Crystals
(Circle all that apply)
Identify the rock (Circle One):
Sandstone
Limestone
Marble
Granite
Gneiss
Describe Your Supporting Evidence:
___________________________________________________________
____________________________________________________________________________________________
____________________________________________________________________________________________
Station 3: Wall of Whitehead Hall
Examine the pale beige rock that covers the lower walls of Whitehead Hall.
Run your hand along the surface of this unpolished rock. Describe how it feels.
___________________________________________________________________________________________
What are the rusty-orange bands within the pale beige rock?
Bedding
Gneissosity
Identify the pale beige rock:
Sandstone
Stylolite
(Circle One)
Limestone
Marble
Granite
Gneiss
(Circle One)
Describe Your Supporting Evidence:
____________________________________________________________________________________________
____________________________________________________________________________________________
____________________________________________________________________________________________
Station 4: Wall around James Hall
The 3 to 4 foot wall around James Hall is composed of two rocks. Most of the wall is covered with a pale beige rock.
The lowest 6 to 12 inches of the wall is composed of a multi-colored rock. Examine these two rocks and answer the
following questions:
Examine the components that comprise the beige rock. What are the grains? Sketch characteristic examples.
Sand
Fossils
Crystals
(Circle all that apply)
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Is the beige rock metamorphosed?
Yes
No
(Circle One)
Describe Your Supporting Evidence:
____________________________________________________________________________________________
____________________________________________________________________________________________
____________________________________________________________________________________________
Identify the beige rock:
Sandstone
Limestone
Marble
Granite
Gneiss
(Circle One)
Describe Your Supporting Evidence:
____________________________________________________________________________________________
____________________________________________________________________________________________
____________________________________________________________________________________________
Examine the grains within the multi-colored rock at the base of the wall.
What are the grains? Sketch characteristic grains.
Sand
Fossils
Crystals
Has this rock been metamorphosed?
(Circle all that apply)
Yes
No
(Circle One)
Identify the beige rock (Circle One):
Sandstone
Limestone
Marble
Granite
Gneiss
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Describe Your Supporting Evidence:
____________________________________________________________________________________________
____________________________________________________________________________________________
____________________________________________________________________________________________
Which of the two rocks in this wall is more resistant to weathering and erosion?
Top of Wall
Base of Wall
(Circle One)
Describe Your Supporting Evidence:
____________________________________________________________________________________________
____________________________________________________________________________________________
____________________________________________________________________________________________
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